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城市喀斯特区水资源可持续管理的水文模型。

Hydrologic Modeling for Sustainable Water Resources Management in Urbanized Karst Areas.

机构信息

Departamento de Geografia, Universidade Federal de Minas Gerais, Av. Antônio Carlos, 6.627 Pampulha, Belo Horizonte 31270-901, Minas Gerais, Brazil.

EMBRAPA Milho e Sorgo, Rodovia MG-424, Km 45 Caixa Postal: 285 ou 151, Sete Lagoas 35701-970, Minas Gerais, Brazil.

出版信息

Int J Environ Res Public Health. 2019 Jul 16;16(14):2542. doi: 10.3390/ijerph16142542.

Abstract

The potential of karst aquifers as a drinking water resource is substantial because of their large storage capacity gained in the course of carbonate dissolution. Carbonate dissolution and consequent development of preferential paths are also the reasons for the complex behavior of these aquifers as regards surface and underground flow. Hydrological modeling is therefore of paramount importance for an adequate assessment of flow components in catchments shaped on karsts. The cross tabulation of such components with geology, soils, and land use data in Geographic Information Systems helps decision makers to set up sustainable groundwater abstractions and allocate areas for storage of quality surface water, in the context of conjunctive water resources management. In the present study, a hydrologic modeling using the JAMS J2000 software was conducted in a karst area of Jequitiba River basin located near the Sete Lagoas town in the state of Minas Gerais, Brazil. The results revealed a very high surface water component explained by urbanization of Sete Lagoas, which hampers the recharge of 7.9 hm yr of storm water. They also exposed a very large negative difference (-8.3 hm yr) between groundwater availability (6.3 hm yr) and current groundwater abstraction from the karst aquifer (14.6 hm yr), which is in keeping with previously reported water table declines around drilled wells that can reach 48 m in old wells used for public water supply. Artificial recharge of excess surface flow is not recommended within the urban areas, given the high risk of groundwater contamination with metals and hydrocarbons potentially transported in storm water, as well as development of suffosional sinkholes as a consequence of concentrated storm flow. The surface component could however be stored in small dams in forested areas from the catchment headwaters and diverted to the urban area to complement the drinking water supply. The percolation in soil was estimated to be high in areas used for agriculture and pastures. The implementation of correct fertilizing, management, and irrigation practices are considered crucial to attenuate potential contamination of groundwater and suffosional sinkhole development in these areas.

摘要

岩溶含水层作为饮用水资源的潜力很大,因为它们在碳酸盐溶解过程中获得了大量的储存能力。碳酸盐溶解和随之而来的优先路径的发展也是这些含水层在地表水和地下水流动方面表现出复杂行为的原因。因此,水文模型对于对岩溶地貌流域中的水流成分进行充分评估至关重要。在地理信息系统中,将这些成分与地质、土壤和土地利用数据进行交叉制表,有助于决策者在联合水资源管理的背景下,为可持续的地下水抽取和优质地表水储存分配区域。在本研究中,在巴西米纳斯吉拉斯州塞特罗拉斯镇附近的杰奎蒂巴河流域的岩溶地区使用 JAMS J2000 软件进行了水文模型模拟。结果表明,由于塞特罗拉斯的城市化,地表水成分非常高,阻碍了 7.9 hm yr 的暴雨水的补给。它们还暴露了一个非常大的负差异(-8.3 hm yr),即地下水的可利用性(6.3 hm yr)与从岩溶含水层中当前抽取的地下水(14.6 hm yr)之间的差异,这与先前报道的围绕钻井的地下水位下降是一致的,在旧的用于公共供水的水井中,地下水位下降可达 48 米。由于潜在的金属和碳氢化合物在暴雨水输送过程中可能会污染地下水,以及集中的暴雨水流会导致窒息性陷坑的形成,因此不建议在城市地区进行多余的地表水流人工补给。然而,可以在集水区源头的森林地区修建小型水坝来储存地表水流,并将其引至城市地区,以补充饮用水供应。估计在用于农业和牧场的地区土壤的渗透性能很高。实施正确的施肥、管理和灌溉措施被认为是至关重要的,以减轻这些地区的地下水潜在污染和窒息性陷坑的发展。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/689c/6678514/e94850cf6506/ijerph-16-02542-g001.jpg

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